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The term "remineralization" is used in several contexts across different disciplines. The term is most commonly used in the medicinal and physiological fields, where it describes the development or redevelopment of mineralized structures in organisms such as teeth or bone.
Remineralization is a natural process and does not have to involve fluoride. Tooth remineralization is the natural repair process for non-cavitated tooth lesions, [1] [2] in which calcium, phosphate and sometimes fluoride ions are deposited into crystal voids in demineralised enamel. Remineralization can contribute towards restoring strength ...
Mineralization may refer to: . Biomineralization (mineralization in biology), when an inorganic substance precipitates in an organic matrix . Mineralized tissues are tissues that have undergone mineralization, including bones, teeth, antlers, and marine shells
In soil science, mineralization is the decomposition (i.e., oxidation) of the chemical compounds in organic matter, by which the nutrients in those compounds are released in soluble inorganic forms that may be available to plants.
Destroyed tooth structure does not fully regenerate, although remineralization of very small carious lesions may occur if dental hygiene is kept at optimal level. [15] For the small lesions, topical fluoride is sometimes used to encourage remineralization. For larger lesions, the progression of dental caries can be stopped by treatment.
Remineralisation (UK spelling; US remineralization) is the transformation of organic molecules to inorganic forms. Remineralisation may also refer to: Bone remodeling (bone metabolism) Remineralisation of teeth; Rockdust, also known as soil remineralization when applied as a nonsynthetic organic fertilizer
Fossil skeletal parts from extinct belemnite cephalopods of the Jurassic – these contain mineralized calcite and aragonite.. Biomineralization, also written biomineralisation, is the process by which living organisms produce minerals, [a] often resulting in hardened or stiffened mineralized tissues.
It has been shown that phytoplankton play a key role in helping maintain this ratio. As organic matter sinks both nitrate and phosphate are released into the ocean via remineralization. Microorganisms preferentially consume oxygen in nitrate over phosphate leading to deeper oceanic waters having an N:P ratio of less than 16:1.